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Fire Ecology of Ponderosa Pine and the Rebuilding of Fire-Resilient Ponderosa Pine Ecosystems 1

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Fire Ecology of Ponderosa Pine and the Rebuilding of Fire-Resilient Ponderosa Pine Ecosystems 1 Stephen A. Fitzgerald2 Abstract The ponderosa pine ecosystems of the West have change dramatically since Euro-American settlement 140 years ago due to past land uses and the curtailment of natural fire. Today, ponderosa pine forests contain over abundance of fuel, and stand densities have increased from a range of 49-124 trees ha-1 (20-50 trees acre-1) to a range of 1235-2470 trees ha-1 (500 to 1000 stems acre-1). As a result, long-term tree, stand, and landscape health has been compromised and stand and landscape conditions now promote large, uncharacteristic wildfires. Reversing this trend is paramount. Improving the fire-resiliency of ponderosa pine forests requires understanding the connection between fire behavior and severity and forest structure and fuels. Restoration treatments (thinning, prescribed fire, mowing and other mechanical treatments) that reduce surface, ladder, and crown fuels can reduce fire severity and the potential for high-intensity crown fires. Understanding the historical role of fire in shaping ponderosa pine ecosystems is important for designing restoration treatments. Without intelligent, ecosystem-based restoration treatments in the near term, forest health and wildfire conditions will continue to deteriorate in the long term and the situation is not likely to rectify itself. Introduction Historically, ponderosa pine ecosystems have had an intimate and inseparable relationship with fire. No other disturbance has had such a re-occurring influence on the development and maintenance of ponderosa pine ecosystems. Historically this relationship with fire varied somewhat across the range of ponderosa pine, and it varied temporally in concert with changes in climate. Over the last century this relationship has undergone an increasing amount of strain. Although wildfires continue to burn in ponderosa pine ecosystems, recent wildfires tend to be more intense and lethal, and consume large expanses of ponderosa pine forests. There is an impending need to better understand the role of fire and techniques land managers can use to emulate fire to restore fire-resiliency. I define fire-resiliency simply as the ability of ponderosa pine forests to survive wildfires relatively intact, as typically occurred during presettlement times. 1 An abbreviated version of this paper was presented at the symposium on Ponderosa Pine: Issues, Trends and Management, October 18-21, 2004, Klamath Falls, Oregon. 2 Professor and Silviculture and Wildland Fire Education Specialist, Oregon State University Extension Forestry Program, Central Oregon Region, 3893 SW Airport Way, Redmond, OR 97756 (email: [email protected]) USDA Forest Service Gen. Tech. Rep. PSW-GTR-198. 2005. 197 Fire ecology of ponderosa pine – fire resilient ponderosa pine ecosystems -- Fitzgerald This paper discusses the ecological role of fire in ponderosa pine ecosystems, changes in forest structure and fire behavior over the past century, and strategies for rebuilding fire-resilience in ponderosa pine ecosystems in western North America. Adaptations and Morphological Characteristics Affecting Fire Resistance and Survival Various adaptations allow vegetation to survive fire. Adaptations can either facilitate survival of species (e.g., fire-stimulated flowering, refractory seed buried in soils, etc) or individuals (e.g. thick bark, basal sprouting, etc) (Kauffman 1990). Ponderosa pine is considered one the most fire resistant conifers in the west, and fire resistance increases as the tree matures (Miller 2000). Ponderosa pine is well suited to survive low-intensity surface fires primarily due to its bark characteristics. Ponderosa pine develops a protective outer corky bark (0.3-0.6 cm) early in life when saplings reach a basal diameter of 5 cm allowing some young trees to survive very light-intensity surface fires (Figure 1a) (Hall 1980). Mature ponderosa pine trees possess thick, exfoliating bark (Figure 1b), which slough off when the bark is on fire. Presumably, this helps “take away” heat as flaming bark flecks flake off, thus reducing or preventing heat transfer and minimizing injury to cambial cells; however, this mechanism has not been well researched. Ponderosa pine bark on mature trees continues to flake off with or without fire, and over long time periods without fire a thick mulch layer of bark develops at the base of trees. When ignited, this mulch smolders for days, conveying heat directly to and through the bark to the cambial layer, often killing or severely stressing the tree. Bark beetles may then attack and kill weakened trees. Historically, frequent low-intensity surface fires prevented this bark mulch layer from accumulating around mature trees. Ponderosa pine also has a deep rooting habit compared to other western conifer species (e.g., true firs, Engelmann spruce, and lodgepole pine). Although a surface fire may heat the soil and kill some surface roots, deeper roots remain intact and allow for continued uptake of water and nutrients. The amount and moisture content of surface fuels (needles and branches, saplings and herbaceous plant material) along with larger woody debris (downed logs) beneath or in contact with the tree affects the degree of injury to surface roots. Ponderosa pine crown structure, branching pattern, and needle and bud characteristics also affect survival during fire. The open crown structure and branching pattern of ponderosa pine allows for better mixing of air and dissipation of heat within stands during a fire, thus reducing the potential for crown scorch. The open crown structure may also dampen fire-spread through tree crowns in less extreme fire conditions (Flint 1925, Agee 1993). Ponderosa pine has long needles with high moisture content that surround terminal buds. Although needles may be scorched and killed by heat, they help protect meristematic tissue within the bud, allowing branch tips to refoliate. Buds of ponderosa pine have thick outer scales that also help protect meristematic tissue from heat (Miller 2000). 198 USDA Forest Service Gen. Tech. Rep. PSW-GTR-198.2005. Fire ecology of ponderosa pine – fire resilient ponderosa pine ecosystems -- Fitzgerald A B Figure 1—(A) This young ponderosa pine survived a light-intensity surface fire when the basal diameter was about 3-4 cm. Note that the cambium on approximately half the circumference was killed. The sapling recovered and greatly accelerated its diameter growth probably as a result of less competition and a flush of nutrients following the fire. (B)Typical fire-resistant bark of an old-growth ponderosa pine showing the platy bark surface. Another factor reportedly affecting fire resistance is ponderosa pine’s ability to self-prune (gradual shedding of lower branches) (Flint 1925, Starker 1934, Miller 2000), resulting in the clear bole that often characterizes large-diameter old-growth ponderosa pine. Presumably, this mechanism lifts the lower crown over time and prevents surface fires from moving up into the tree’s canopy. However, there is no evidence that ponderosa pine self-prunes on its own. The clear boles are a result of USDA Forest Service Gen. Tech. Rep. PSW-GTR-198.2005. 199 Fire ecology of ponderosa pine – fire resilient ponderosa pine ecosystems -- Fitzgerald either repeated surface fires, which scorch and kill lower branches when trees are young and lower branches have small diameters, and/or death of lower branches from competition (shading) from neighboring trees. In both cases, dead branches are shed and remaining stubs are grown over after decades or centuries of tree growth. Evidence that counters the notion of self-pruning is demonstrated by open-grown ponderosa pine in areas where fires were naturally excluded, such as in rocky areas where fuels are too scarce to carry fire. Often these trees have branches that are large, heavy, and located on the lower portions of the bole showing no propensity for self-pruning. Fire Regimes in Ponderosa Pine Ecosystems Fire regimes are influenced greatly by climate, vegetation types and by topographic and geologic features that either facilitate or restrict fire spread (Agee 1993, Camp and others1997, Taylor and Skinner 1998). Fire regimes are characterized by their frequency, intensity, severity, extent, and seasonality and have a great influence on vegetative recovery, plant succession, and forest and ecosystem structure (Agee 1993). Frequency Fire frequency, or the mean fire return interval, is a measure of how often fire returns, on average, to an area. There may be a wide range around this mean, which has important ecological implications for stand development and forest structure (Baker and Ehle 2001). The median fire return interval is also used to characterize fire return intervals in forest ecosystems. Within ponderosa pine ecosystems, fire returned approximately every 2-47 years. This estimate of fire frequency is based on several studies that date fire scars on individual trees (point sample) or from several fire-scarred trees in an area (composite fire interval) (Table 1). The wide range in fire frequency is a reflection of current and past regional climate, plant association, aspect and slope, elevation, aboriginal burning and other factors. In the Front Range of Colorado, for example, ponderosa pine forests were subject to frequent surface fires at lower elevations, much like other ponderosa pine forests in the west. At higher elevations (2400 m), where ponderosa pine is mixed with Douglas-fir and lodgepole pine (more moist conditions), fires were less frequent and were a combination of both surface and stand-replacing fire (Veblen and others 2000). In western Montana, Arno and others (1997) observed the same change in fire frequency from pure ponderosa pine stands to more mesic mixed stands of ponderosa pine and western larch. Other studies have shown a link between regional climate patterns, such as periods of wet and dry (drought) conditions and fire occurrence (Swetnam 1988, Touchman and others 1996, Veblen and others 2000, Grissino-Mayer and others 2004, Wright and Agee 2004). Lightning is thought to have been the primary source of presettlement fire ignitions.
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